The distribution of active faults in the Iberian Peninsula is not homogeneous, being mainly
present, but not only, in areas affected by the Alpine Orogeny. They are located in several …

We present the first GPS‐derived geodetic observations from the NE end of the Eastern
Betic Shear Zone obtained from the Bajo Segura GPS network (SE Spain). The network has …

The low frequency of large destructive earthquakes in the Eastern Betics (SE Iberian
Peninsula), not recorded in the instrumental seismic catalog, complicate the estimation of …

Abstract The Bajo Segura basin (eastern Betic Cordillera) has one of the most complete late
Miocene–early Pliocene marine records of the western Mediterranean. An updated …

Trying to decipher how paleoseismic activity has influenced the altitudinal disposition of
interglacial deposits is one of the main challenges to be confronted before quantifying …

Abstract Interpretation of new multichannel seismic reflection profiles indicates that the
Palomares margin was formed by crustal‐scale extension and coeval magmatic accretion …

Including faults as seismogenic sources in probabilistic seismic hazard assessments
(PSHA) has turned into a common practice as knowledge of active faults is improving …

Recently acquired swath-bathymetry data and high-resolution seismic reflection profiles
offshore Adra (Almería, Spain) reveal the surficial expression of a NW–SE trending 20 km …

The present paper introduces a new risk-informed based tool that can support disaster
management authorities in making decisions in response to earthquakes at local and …

Fault slip rate variability over time is a crucial aspect for understanding how single faults
interact among each other in fault systems. Several studies worldwide evidence the …